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SWEAT SPIRE

Mountains and Summits


Pacific Ranges Olympic Mountains

Sweat Spire

7,580 ft

Sweat Spire, located in the Pacific Ranges mountain range, is a prominent peak with an elevation of [elevation]. This majestic mountain offers a challenging climb for mountaineers, attracting adventurers from around the world.

During the winter season, Sweat Spire experiences significant snowfall, resulting in a diverse and dynamic snowpack range. From lower elevations to the summit, climbers encounter varying degrees of snow accumulation, making it essential for mountaineers to assess avalanche hazards and plan their ascent accordingly. The changing snowpack conditions require climbers to possess advanced skills and knowledge of snow stability and avalanche safety.

Sweat Spire contributes to the hydrology of the region, with its melting snow providing runoff to several creeks and rivers in the surrounding area. These waterways, such as [specific creek/river names], benefit from the mountain's meltwater, providing crucial resources for wildlife and ecosystems downstream.

The name "Sweat Spire" holds an intriguing history and is believed to derive from [lore or legend]. While the exact origin may vary depending on different sources, the name adds an element of mystique to the mountain. Exploring the lore and legends surrounding Sweat Spire adds to the allure for mountaineers and outdoor enthusiasts seeking a memorable adventure in the Pacific Ranges.


Regional Water Data

Gauge Streamflow Stage
Wynoochee River Above Black Creek Nr Montesano
USGS 12037400
507 cfs 27.8 ft
Big Quilcene River Below Diversion Nr Quilcene
USGS 12052210
80 cfs 1.4 ft
Wynoochee River Above Save Creek Near Aberdeen
USGS 12036000
384 cfs 5.0 ft
North Fork Skokomish River Near Potlatch
USGS 12059500
268 cfs 3.0 ft
Skokomish River Near Potlatch
USGS 12061500
698 cfs 13.7 ft
Elwha River Above Lake Mills Nr Port Angeles
USGS 12044900
725 cfs 539.3 ft
South Fork Skokomish River Near Union
USGS 12060500
281 cfs 0.6 ft
Snotel Site Snowpack 24hr Change

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